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Overview of the Holocene History, Architecture, and Structural Components of Tague Reef and Lagoon Overview of the Holocene History, Architecture, and Structural Components of Tague Reef and Lagoon Randolph Burke Walter Adey Ian MacIntyre Converted to digital format by Thomas F. Barry (NOAA/RSMAS) in 2004. Copy available at the NOAA Miami Regional Library. Minor editorial changes may have been made. 105 Overview of the Holocene History, Architecture, and Structural Components of Tague Reef and Lagoon Randolph B. Burkel , Walter H. Adey2, and Ian G. MacIntyre2 1North Dakota Geological Survey, P.O. Box 8156, Grand Forks, ND 2Smithsonian Institution, Division of Paleobotany, Washington D.C INTRODUCTION backreef at both the eastern and western ends of the reef tract. Seaward of the main barrier, Buck Island Channel This paper presents a synopsis of the data from two deepens to the east from a shallow depth of 8 m north of coring programs that investigated Tague Reef off the Sand Cay to 20 m north of Boiler Bay. Channel Rock, at northeast coast of St. Croix. This 7.8-km-long bank- the eastern end of Buck Island Channel, defines the crest of barrier reef, located between Pull Point to the west and another elongate reef that parallels Tague reef and shoals Lamb Point to the east (Fig. 1), is situated on the St. to a depth of less than 2 m (Fig. 1). Croix insular platform, over 2 km from the shelf edge. The zonation pattern of the reef community generally The bank-barrier reef (Adey, 1975) is one geologic type parallels the reef trend. The lagoon is characterized by belonging to the basic tripartite reef system of St. Croix seagrasses and sediment-dwelling organisms dominated by (Adey and Burke, 1976; Adey, 1978) that also includes molluscs and echinoderms. Calcareous algae are, for the fringing and shelf-edge reefs (Adey et al., 1977b). most part, dominated by Penicillus sp. and a variety of Halimeda spp. The abrupt transition from the lagoon to Setting the backreef is marked by scattered corals (particularly The shoreline behind Tague Reef is characterized by Montastrea annularis and Porites), gorgonians, and a arcuate bays with skeletal sand beaches and rocky variety of fleshy algae. The reef crest is distinguished by headlands. At some locations, such as in portions of a diverse, mixed coral community including Acropora Boiler Bay, the sand is cemented to form beach rock. palmata and Porites asteroides, with the seaward portion Colluvial deposits occur behind most beaches and flank occupied largely by Acropora palmata and the hydrozoan headlands. Headlands are formed by highly indurated, deep Millepora sp. The shallow forereef typically supports marine sediments of the Cretaceous Caledonia Formation. stands of Acropora palmata, which give way in the deeper Tague Reef has an essentially linear east-west trend forereef to P. porites, A. cervicornis, M. annularis, and that does not follow the promontories of the adjacent Diploria spp. These various living corals are not the shoreline. As a result, the distance between the reef and primary structural components of the reef crest; sediment shore is highly variable, ranging from a maximum of 0.9 and rubble cover more area and volume than do the living km at its western end, to nothing where it fringes against corals. Additional detailed information about the character the shore at Lamb Point. The reef crest is continuous at a of Tague reef are presented in Muller and Gerhard (1974), depth of generally less than 0.5 m (mean low water) from Dahl et at, and Adey et at. (1977a). The relationship of Solitude Bay in the west to Cottongarden Bay in the east. Caribbean reef framework components to environmental West of Solitude Bay the reef becomes segmented into a factors of shelf depth, energy, and water quality are sublinear series of patch reefs; the westernmost segment diagrammatically summarized in Adey and Burke (1977). forms a fringing reef around Sand Cay. East of Cotton- garden Bay the reef crest is generally deeper and wider, and METHODS the reef is broken into broad patch reefs. A few deep (approximately 2.5 m), tortuous sand channels pass Cores were collected from the reef crest with a through the crest at Boiler Bay. The crest shoals at the portable rotary drill mounted on a platform above the reef. eastern end of Boiler Bay forming a broad, shallow A submersible drill was used to obtain cores from deeper- fringing reef. water sites in the lagoon and on the forereef. Notes were Lagoon depths range from a maximum of made on the drilling character every 1.5 m, with emphasis approximately 8 m west of Tague Point to 1 m in the on the depth at which hard substrates were contacted, the 106 Figure 1 . Location map of Tague Reef, St. Croix, U.S.V.I. with core locations numbered. Line A-A' connects the cores taken in a transect from the lagoon to the forereef. Line B-B' connects the cores taken along the reef crest. Place name abbreviations: BB = Boiler Bay, CB = Cottongarden Bay, CR = Channel Rock, SB = Solitude Bay, TB = Tague Bay, TP = Tague Point, and WIL = West Indies Lab. rates of drilling, and the ease of penetration. Sediment coralline algae were retrieved. In cores collected from the thickness was determined in some instances by probing backreef, the sequence of reef development began with for hard substrate with a steel rod. head corals that locally colonized the pre-Holocene surface Each core was examined macroscopically to identify (Fig. 2). Acropora palmata then replaced the head corals the major components (e.g., coral species, sediment, and further reef development consisted of alternating head cements). Thin sections were made of 51 samples, to coral and A. palmata growth as the reef prograded seaward. confirm composition and to assess diagenesis. The reef was capped by a mixed reef community including Radiocarbon dating of 12 samples was used to determine A. palmata and M. annularis. In contrast, cores taken at the age of the reef, accretion rates, and the timing and the reef crest reveal that reef development usually began sequence of reef development. Additional samples were with either A. palmata or head corals colonizing sediment examined by X-ray diffraction to help define the boundary bottoms as opposed to hard substrate. After A. palmata between Holocene and pre-Holocene based on the presence became established at a particular site, it was usually of low-magnesium calcite. overgrown by a mixed coral community that included Millepora sp. and coralline algae which presently cap the RESULTS outer edge of the reef crest. Along the reef crest, pre-Holocene limestone was Fourteen cores were recovered from the locations recovered in three cores, and the pre-Holocene contact was along the reef crest. Nine additional cores were taken at located with a probe in another core hole after collapse of six different locations along a transect from the lagoon to sand into its base. The pre-Holocene contact was the forereef (Fig. 1). Another four cores were taken from established in six cores along the reef transect; in two a patch reef in Cottongarden Bay and one core was taken cores, the underlying unit was colluvium and in four in Tague Bay. others limestone. The colluvium contained angular clasts The major components recovered in the cores were from the Cretaceous Caledonia Formation. The pre- corals (Figs. 2 and 3). Recovery of sediment was poor, Holocene age of the limestone was inferred from its low- resulting in total recoveries of less than 30%. Recovery magnesium calcite mineralogy. was generally greater in the upper, coral-rich portions of A 4-m high bench was found 180 m behind the reef the reef. The lower portions of the cores consisted mostly crest in the pre-Holocene strata beneath Tague Bay (Fig. of sand and rubble with only a few corals. The most 2). Cores taken along transect B-B' indicate that the pre- common corals recovered were Acropora palmata and Holocene contact dips to the east (Fig. 3). Depth to the Montastrea annularis. Lesser amounts of Diploria sp., pre-Holocene limestone along the reef crest ranged from Porites sp., the hydrozoan Millepora sp., and crustose 8.1 m at Sand Cay (core location 12) to 13.8 m off Tague 107 Figure 2. Diagrammatic section of the lagoon to forereef transect (A-A') showing the location of cores, the major components found in the cores, the Holocene-pre-Holocene contact, and radiocarbon dates. Pre-Holocene limestones are shown by the "brick" pattern in this and Figure 3. The position of Neumann s Holocene sea level (Adey, 1975) is indicated on the right margin in thousand-year increments. Note that reef development is seaward of the four-meter-high bench. Bay (core location 17). At Sand Cay, the pre-Holocene current energy and thus trap sediment around them, limestone was overlain by silty clays of unknown age. helping to stabilize the reef structure. The normal Depth of the pre-Holocene contact across the reef transect succession of reef communities from deep to shallow ranged from 4.1 m in the lagoon (core location 1) to 15.5 water is head corals overlain by A. palmata and then m on the forereef (core location 10). mixed corals. Radiocarbon dates ranged from modern to 6,135 ybp The staggered dates for reef development (Fig. 3) ± 80 years. The oldest dates were from A. palmata from suggest that Tague Reef began as a series of isolated core location 17 off Tague Bay. Radiocarbon dates from patches that formed at different times. The patch reefs cores along the reef crest (Fig. 3) revealed that massive grew laterally as sediment and debris infilled between reefs framework components of the reef initiated their growth at and were colonized over time.
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